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Volumn 284, Issue 5417, 1999, Pages 1087-

Considering a neoproterozoic snowball Earth

Author keywords

[No Author keywords available]

Indexed keywords

CARBON DIOXIDE; CARBONIC ACID; SNOW; SURFACE WATER;

EID: 85045340864     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.284.5417.1087a     Document Type: Note
Times cited : (43)

References (24)
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    • (1992) The Proterozoic Biosphere , pp. 51-52
    • Kirschvink, J.L.1
  • 9
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    • Eds., (Cambridge Univ. Press, Cambridge, 1981); Palaeogeogr. Palaeoclimat. Palaeoecol
    • M. J. Hambrey and W. B. Harland, Eds., Earth’s Pre-Pleistocene Glacial Record (Cambridge Univ. Press, Cambridge, 1981); Palaeogeogr. Palaeoclimat. Palaeoecol. 51, 255 (1985);
    • (1985) Earth’S Pre-Pleistocene Glacial Record , vol.51 , pp. 255
    • Hambrey, M.J.1    Harland, W.B.2
  • 12
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    • Norges Geol. Unders. Bull. 394, 1 1984
    • M. B Edwards, Sedimentology 22, 75 (1975); Norges Geol. Unders. Bull. 394, 1 (1984);
    • (1975) Sedimentology , vol.22 , pp. 75
    • Edwards, M.B.1
  • 16
    • 84879654484 scopus 로고
    • in J. B. Anderson and G. M. Ashley, Eds. (Geological Society of America, Spec. Publ. Boulder, CO, )
    • G. M. Young and V. A. Gostin, in Glacial Marine Sedimentation; Paleoclimatic Significance, J. B. Anderson and G. M. Ashley, Eds. (Geological Society of America, Spec. Publ. 261, Boulder, CO, 1991), pp. 207–222.
    • (1991) Glacial Marine Sedimentation; Paleoclimatic Significance , vol.261 , pp. 207-222
    • Young, G.M.1    Gostin, V.A.2
  • 17
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    • marginal areas of sedimentary basins, most glacial sediment accumulates during retreat of the ice sheet
    • In marginal areas of sedimentary basins, most glacial sediment accumulates during retreat of the ice sheet [C. H. Eyles, N. Eyles, A. D. Miall, Palaeogeogr. Palaeoclimat. Palaeoecol. 51, 15 (1985);
    • (1985) Palaeogeogr. Palaeoclimat. Palaeoecol. , vol.51 , pp. 15
    • Eyles, C.H.1    Eyles, N.2    Miall, A.D.3
  • 18
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    • in R. G. Walker and N. James, Eds. (Geological Association of Canada, St. John’s, Canada, )
    • N. Eyles and C. H. Eyles, in Facies Models: Response to Sea Level Change, R. G. Walker and N. P. James, Eds. (Geological Association of Canada, St. John’s, Canada, 1992), pp. 73–100;
    • (1992) Facies Models: Response to Sea Level Change , pp. 73-100
    • Eyles, N.1    Eyles, C.H.2
  • 20
    • 0344762271 scopus 로고    scopus 로고
    • ), ); L. E. Sohl, N. Christie-Blick, D. V. Kent, Geol. Soc. Am. Bull., in press
    • L. E. Sohl, Geol. Soc. Am. Abstr. Programs 29 (no. 6), 195 (1997); L. E. Sohl, N. Christie-Blick, D. V. Kent, Geol. Soc. Am. Bull., in press.
    • (1997) Geol. Soc. Am. Abstr. Programs , vol.29 , Issue.6 , pp. 195
    • Sohl, L.E.1
  • 22
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    • The high concentration of dissolved CO2 would at first have precluded the precipitation of carbonate in the ocean
    • 2 would at first have precluded the precipitation of carbonate in the ocean.
  • 24
    • 85045295853 scopus 로고    scopus 로고
    • We thank Hoffman for the vigorous discussion that his visit inspired
    • We thank and for reviews, and and for discussions. This comment was written following a seminar presented by F. Hoffman at Lamont on 15 January 92-06084, EAR 94-18294, and EAR
    • We thank L. A. Derry and J. Lynch-Stieglitz for reviews, and W. S. Broecker, P. E. Olsen and S. R. Hemming for discussions. This comment was written following a seminar presented by P. F. Hoffman at Lamont on 15 January 1999. We thank Hoffman for the vigorous discussion that his visit inspired. Our research in Neoproterozoic geology has been supported by NSF grants EAR 92-06084, EAR 94-18294, and EAR 96-14070.
    • (1999) Our Research in Neoproterozoic Geology Has Been Supported by NSF Grants EAR , pp. 96-14070
    • Derry, L.A.1    Lynch-Stieglitz, J.2    Broecker, W.S.3    Olsen, P.E.4    Hemming, S.R.5


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